TY  - JOUR
A1  - Öztürk, Ugur
A1  - Marwan, Norbert
A1  - von Specht, Sebastian
A1  - Korup, Oliver
A1  - Jensen, J.
T1  - A new centennial sea-level record for Antalya, Eastern Mediterranean
JF  - Journal of geophysical research-oceans
N2  - Quantitative estimates of sea-level rise in the Mediterranean Basin become increasingly accurate thanks to detailed satellite monitoring. However, such measuring campaigns cover several years to decades, while longer-term sea-level records are rare for the Mediterranean. We used a data archeological approach to reanalyze monthly mean sea-level data of the Antalya-I (1935–1977) tide gauge to fill this gap. We checked the accuracy and reliability of these data before merging them with the more recent records of the Antalya-II (1985–2009) tide gauge, accounting for an eight-year hiatus. We obtain a composite time series of monthly and annual mean sea levels spanning some 75 years, providing the longest record for the eastern Mediterranean Basin, and thus an essential tool for studying the region's recent sea-level trends. We estimate a relative mean sea-level rise of 2.2 ± 0.5 mm/year between 1935 and 2008, with an annual variability (expressed here as the standard deviation of the residuals, σresiduals = 41.4 mm) above that at the closest tide gauges (e.g., Thessaloniki, Greece, σresiduals = 29.0 mm). Relative sea-level rise accelerated to 6.0 ± 1.5 mm/year at Antalya-II; we attribute roughly half of this rate (~3.6 mm/year) to tectonic crustal motion and anthropogenic land subsidence. Our study highlights the value of data archeology for recovering and integrating historic tide gauge data for long-term sea-level and climate studies.
KW  - sea level
KW  - tide gauge
KW  - data archeology
KW  - Mediterranean Sea
Y1  - 2018
U6  - https://doi.org/10.1029/2018JC013906
SN  - 2169-9275
SN  - 2169-9291
VL  - 123
IS  - 7
SP  - 4503
EP  - 4517
PB  - American Geophysical Union
CY  - Washington
ER  - 
TY  - JOUR
A1  - Albrecht, Torsten
A1  - Levermann, Anders
T1  - Spontaneous ice-front retreat caused by disintegration of adjacent ice shelf in Antarctica
JF  - Earth & planetary science letters
N2  - Antarctic ice-discharge constitutes the largest uncertainty in future sea-level projections. Floating ice shelves, fringing most of Antarctica, exert retentive forces onto the ice flow. While abrupt ice-shelf retreat has been observed, it is generally considered a localized phenomenon. Here we show that the disintegration of an ice shelf may induce the spontaneous retreat of its neighbor. As an example, we reproduce the spontaneous but gradual retreat of the Larsen B ice front as observed after the disintegration of the adjacent Larsen A ice shelf. We show that the Larsen A collapse yields a change in spreading rate in Larsen B via their connecting ice channels and thereby causes a retreat of the ice front to its observed position of the year 2000, prior to its collapse. This mechanism might be particularly relevant for the role of East Antarctica and the Antarctic Peninsula in future sea level.
KW  - Antarctica
KW  - Larsen Ice Shelf
KW  - glaciology
KW  - numerical ice modeling
KW  - sea level
KW  - iceberg calving
Y1  - 2014
U6  - https://doi.org/10.1016/j.epsl.2014.02.034
SN  - 0012-821X
SN  - 1385-013X
VL  - 393
SP  - 26
EP  - 30
PB  - Elsevier
CY  - Amsterdam
ER  -